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Observed Seismicity - University of Kentucky

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Discussion<br />

9<br />

Figure 9. Seismic recordings <strong>of</strong> the Bardwell event from station BLKY.<br />

Table 4. Comparison <strong>of</strong> parameters <strong>of</strong> the Bardwell, Ky., and Blytheville, Ark., earthquakes.<br />

Date Time Magnitude Location Focal Depth<br />

(EDT) (M w<br />

) (La./Lo.) (km)<br />

06/06/2003 8:29:34 a.m. 4.0 36.88N/88.98W 2.3<br />

04/30/2003 0:56:22 a.m. 4.0 35.92N/89.92W 23.8<br />

The observed seismicity between January<br />

and June 2003 in the New Madrid Seismic<br />

Zone indicates that (1) most recorded<br />

seismicity in the central United States reflects<br />

the active faults <strong>of</strong> the New Madrid Seismic<br />

Zone and (2) in the Jackson Purchase Region,<br />

characteristics <strong>of</strong> earthquakes, such as focal<br />

depth, are different from those <strong>of</strong> earthquakes<br />

in the central New Madrid Seismic<br />

Zone. Six months <strong>of</strong> seismic monitoring is<br />

not enough time to make a scientifically<br />

defensible conclusion about the extent <strong>of</strong> the<br />

active faults into the Jackson Purchase Region.<br />

Much more time is needed for seismic<br />

monitoring in the area. The observed seismicity<br />

suggests, however, that the active<br />

faults <strong>of</strong> the New Madrid Seismic Zone may<br />

not extend into the Jackson Purchase Region.<br />

This could result in lower estimates <strong>of</strong> the<br />

seismic hazard in western <strong>Kentucky</strong>.

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